about a mile out, tempts us to a delicious morning
draught.
A little further down is "Pap." Church's "Devil's Playground,"
"Devil's Post," and devil's this, that and the other, out of which
he gained considerable satisfaction while driving stage-coach between
Truckee and Tahoe in the days before the railroad.
It is well carefully to observe these singular lava puddingstone
masses, for, according to the theory of John Le Conte, the eminent
physicist, recounted in another chapter, these were the restraining
masses that made the Lake at one time eighty or a hundred feet higher
than it is to-day.
Four miles from the Tavern we pass Engineer Von Schmidt's old dam, for
the history of which see the chapter on "The Truckee River."
Near Deer Park Station is another spring on the right. In the old
stage days "Pap." Church always stopped here and gave his passengers
the opportunity to drink of the water, while he made discourse as to
its remarkable coldness. Five years ago a land slide completely buried
it, and the road had to be cut through again. Ever since the spring
has been partially clogged and does not flow freely, but it is cold
enough to make one's teeth ache.
In the winter of 1881-2 a land-and-snow-slide occurred a little beyond
Deer Park Station. Watson was carrying the mail on snow-shoes at the
time and saw it. There had been a five foot fall of snow in early
March, and a week or two later came a second fall of seven feet.
Something started the mass, and down it came, rushing completely
across the river and damming it up, high on the other side, and the
course of the slide can clearly be seen to-day. It is now, however,
almost covered with recent growth of chaparral, and thus contributed
to one of the most beautiful effects of light and shade I ever saw.
The mountain slope on one side was completely covered with a growth of
perfect trees. Through these came pencillings of light from the rising
sun, casting alternate rulings of light and shadow in parallel lines
on the glossy surface of the chaparral beyond. The effect was enhanced
by the fleecy and sunshiny clouds floating in the cobalt blue above.
Near the mouth of Bear Creek the river makes a slight curve and also
a drop at the same time, and the road, making a slight rise, presents
the view of a beautiful stretch of roaring and foaming cascades.
Here the canyon walls are of bare, rocky ridges, of white and red
barrenness, with occasional patches of timb
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